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不透水表面下贫瘠的土壤碳氮库。

Depleted soil carbon and nitrogen pools beneath impervious surfaces.

机构信息

Boston University, Department of Geography & Environment, Boston, MA, USA.

出版信息

Environ Pollut. 2012 May;164:248-51. doi: 10.1016/j.envpol.2012.01.046. Epub 2012 Feb 28.

Abstract

Urban soils and vegetation contain large pools of carbon (C) and nitrogen (N) and may sequester these elements at considerable rates; however, there have been no systematic studies of the composition of soils beneath the impervious surfaces that dominate urban areas. This has made it impossible to reliably estimate the net impact of urbanization on terrestrial C and N pools. In this study, we compared open area and impervious-covered soils in New York City and found that the C and N content of the soil (0-15 cm) under impervious surfaces was 66% and 95% lower, respectively. Analysis of extracellular enzyme activities in the soils suggests that recalcitrant compounds dominate the organic matter pool under impervious surfaces. If the differences between impervious-covered and open area soils represent a loss of C and N from urban ecosystems, the magnitude of these losses could offset sequestration in other parts of the urban landscape.

摘要

城市土壤和植被含有大量的碳(C)和氮(N),并且可能以相当高的速率将这些元素固定;然而,对于主导城市地区的不透水表面下土壤的组成,还没有进行过系统的研究。这使得无法可靠地估计城市化对陆地碳和氮库的净影响。在这项研究中,我们比较了纽约市的开放区域和不透水覆盖区域的土壤,发现不透水表面下土壤(0-15 厘米)中的碳和氮含量分别低了 66%和 95%。对土壤中细胞外酶活性的分析表明,在不透水表面下,难降解化合物占据了有机物质库的主导地位。如果不透水覆盖区域和开放区域土壤之间的差异代表了城市生态系统中碳和氮的损失,那么这些损失的规模可能会抵消城市景观其他部分的固定。

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